Lecture Outlines PowerPoint Chapter 14 Tarbuck/Lutgens€¦ · Composition of seawater Seawater consists of about 3.5% (by weight) dissolved minerals Salinity •Total amount of solid

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Lecture Outlines

PowerPoint

Chapter 14

Earth Science 11e

Tarbuck/Lutgens

Earth Science, 11e

Ocean Water and

Ocean Life

Chapter 14

Composition of seawater

Seawater consists of about 3.5% (by

weight) dissolved minerals

Salinity

• Total amount of solid material dissolved in

water

• Typically expressed in parts-per-thousand (‰)

• Average salinity is 35‰

• Major constituent is sodium chloride

Relative proportions of

water and dissolved

components in seawater

Figure 14.1


Sources of sea salts

• Chemical weathering of rocks

• Outgassing – gases from volcanic eruptions

Processes affecting seawater salinity

• Variations in salinity are a consequence of

changes in the water content of the solution



• Processes that decrease salinity (add water)

• Precipitation

• Runoff from land

• Icebergs melting

• Sea ice melting

• Processes that increase salinity (remove water)

• Evaporation

• Formation of sea ice



• Surface salinity in the open ocean ranges from

33‰ to 38‰

Ocean temperature

Surface water temperature varies with the

amount of solar radiation received

• Lower surface temperatures are found in high-

latitude regions

• Higher temperatures found in low-latitude

regions

Ocean temperature

Temperature variation with depth

• Low-latitudes

• High temperature at the surface

• Rapid decrease in temperature with depth

(thermocline)

• High-latitudes

• Cooler surface temperatures

• No rapid change in temperature with depth

Variations in ocean water

temperature with depth

Figure 14.4

Ocean temperature

Ocean temperature over time

• The unique thermal properties of seawater

make it resistant to temperature changes

• Global warming could eventually influence

ocean temperatures

Variations in the ocean’s surface

temperature and

salinity with latitude

Figure 14.3

Ocean density

Density is mass per unit volume - how

heavy something is for its size

Determines the water’s vertical position in

the ocean

Factors affecting seawater density

• Salinity

• Temperature - the greatest influence

Ocean density

Variations with depth

• Low-latitudes

• Low density at the surface

• Density increases rapidly with depth (pycnocline)

because of colder water

• High-latitudes

• High-density (cold) water at the surface

• Little change in density with depth

Variations in ocean water

density with depth

Figure 14.5

Ocean density

Ocean layering

• Layered according to density

• Three-layered structure

• Surface mixed zone

• Sun-warmed zone

• Zone of mixing

• Shallow (300 meters)

Ocean density

Ocean layering

• Three-layered structure

• Transition zone

• Between surface layer and deep zone

• Thermocline and pycnocline

• Deep zone

• Sunlight never reaches this zone

• Temperatures are just a few degrees above

freezing

• Constant high-density water

Layering in the ocean

Figure 14.6

Ocean life

Marine environment is inhabited by a wide

variety of organisms

Most organisms live within the sunlight

surface waters (photosynthesis)

Classification of marine organisms

• Plankton

• Floaters

• Algae (phytoplankton)

Ocean life


• Plankton

• Animals (zooplankton)

• Bacteria

• Most of Earth’s biomass

• Nekton

• All animals capable of moving independently of the

ocean currents

• They are unable to move throughout the breath of

the ocean

Ocean life


• Benthos

• Bottom dwellers

• A great number of species exist on the shallow

coastal floor

• Most live in perpetual darkness in deep water

Ocean life

Marine life zones

• Several factors are used to divide the ocean into

distinct marine life zones

• Availability of light

• Photic (light) zone

• Upper part of ocean

• Sunlit

• Euphotic zone is near the surface where the

light is strong

Ocean life

Marine life zones



• Availability of light

• Aphotic (without light) zone

• Deep ocean

• No sunlight

Ocean life

Marine life zones



• Distance from shore

• Intertidal zone – area where land and ocean meet

and overlap

• Neritic zone – seaward from the low tide line,

the continental shelf out to the shelf break

• Oceanic zone – beyond the continental shelf

Ocean life

Marine life zones

• Several factors are used to divide the ocean into distinct marine life zones

• Water depth

• Pelagic zone – open ocean of any depth

• Benthic zone – includes any sea-bottom surface

• Abyssal zone – a subdivision of the benthic zone

• Deep

• Extremely high water pressure

• Low temperatures

Ocean life

Marine life zones



• Water depth

• Abyssal zone – a subdivision of the benthic zone

• No sunlight

• Sparse life

• Food sources include decaying particles

from above, large fragments falling, and

hydrothermal vents

Marine life zones

Figure 14.10

Oceanic Productivity

Related to primary productivity

• The amount of carbon fixed by organisms

through the synthesis of organic matter

• Sources of energy

• Photosynthesis (solar radiation)

• Chemosynthesis (chemical reactions)

• Influenced by

• Availability of nutrients

• Amount of solar radiation


Related to primary productivity

• Most abundant marine life exists where there is

ample

• Nutrients

• Good sunlight

Productivity in polar oceans

• Because of nutrients rising from deeper water,

high-latitude surface waters have high nutrient

concentrations


Productivity in polar oceans

• Low solar energy limits photosynthetic

productivity

Productivity in tropical oceans

• Low in the open ocean

• Thermocline eliminates the supply of nutrients

from deeper waters below

An example of productivity in

polar oceans (Barents Sea)

Figure 14.11

Productivity in tropical oceans

Figure 14.12


Productivity in temperate oceans

• Winter

• Low productivity

• Days are short and sun angle is low

• Spring

• Spring bloom of phytoplankton is quickly depleted

• Productivity is limited



• Summer

• Strong thermocline develops so surface nutrients are not replaced from below

• Phytoplankton population remains relatively low

• Fall

• Thermocline breaks down and nutrients return to the surface

• Short-lived fall bloom of phytoplankton

Highest overall productivity occurs in temperate regions


(Northern Hemisphere)

Figure 14.13

Oceanic feeding relationships

Main oceanic producers

• Marine algae

• Plants

• Bacteria

• Bacteria-like archaea

Only a small percentage of the energy taken

in at any level is passed on to the next


Trophic levels

• Chemical energy stored in the mass of the

ocean’s algae is transferred to the animal

community mostly through feeding

• Each feeding stage is called a trophic level

Transfer of energy between trophic levels is

very inefficient (about 2%)

Ecosystem energy flow

and efficiency

Figure 14.15


Food chains and food webs

• Food chain - a sequence of organisms through

which energy is transferred

• Food web

• Involves feeding on a number of different animals

• Animals that feed through a food web rather than a

food chain are more likely to survive

Comparison between a food

chain and a food web

Figure 14.16

End of Chapter 14

Documents

Lecture Outlines PowerPoint Chapter 14 Tarbuck/Lutgens€¦ · Composition of seawater Seawater consists of about 3.5% (by weight) dissolved minerals Salinity •Total amount of solid